Possible Settling of Perennially Frozen Loose Deposits in West Siberia during Thawing (Vozmoshnye Osadki pri Profaivanii Mnogelet Nemerzlykh Sibir)
In the development of land with perennially frozen friable deposits of great depth, a serious danger is presented by the thermal settlings of buildings erected on high-ice soils. Therefore a knowledge of the amounts of possible settlings permits the builder to form a rough judgment concerning the su...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1972
|
Subjects: | |
Online Access: | http://www.dtic.mil/docs/citations/AD0738127 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0738127 |
id |
ftdtic:AD0738127 |
---|---|
record_format |
openpolar |
spelling |
ftdtic:AD0738127 2023-05-15T16:37:01+02:00 Possible Settling of Perennially Frozen Loose Deposits in West Siberia during Thawing (Vozmoshnye Osadki pri Profaivanii Mnogelet Nemerzlykh Sibir) Dubikov,G. I. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1972-01 text/html http://www.dtic.mil/docs/citations/AD0738127 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0738127 en eng http://www.dtic.mil/docs/citations/AD0738127 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Civil Engineering (*SOILS DEFORMATION) (*PERMAFROST SOILS) FOUNDATIONS(STRUCTURES) CONSTRUCTION ICE MELTING FREEZING MOISTURE TABLES(DATA) SIBERIA USSR TRANSLATIONS Text 1972 ftdtic 2016-02-19T01:24:51Z In the development of land with perennially frozen friable deposits of great depth, a serious danger is presented by the thermal settlings of buildings erected on high-ice soils. Therefore a knowledge of the amounts of possible settlings permits the builder to form a rough judgment concerning the suitability or unsuitability of soils as a foundation for construction and to recommend a building technique even during the initial stage of studies. Since during thawing, the settlings are determined by the extent of ice saturation of the frozen friable deposits, while iciness is linked largely with the lithological composition and method of freezing the soils, the values of possible settlings also depend on these factors. The report gives values of possible settlings during the thawing of the upper levels of frozen Quaternary deposits in Western Siberia. (Author) Draft trans. of Merzlotnye Issledovaniya (USSR) n10 p220-222 1970. Text Ice permafrost Siberia Defense Technical Information Center: DTIC Technical Reports database Sibir’ ENVELOPE(158.683,158.683,68.500,68.500) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Civil Engineering (*SOILS DEFORMATION) (*PERMAFROST SOILS) FOUNDATIONS(STRUCTURES) CONSTRUCTION ICE MELTING FREEZING MOISTURE TABLES(DATA) SIBERIA USSR TRANSLATIONS |
spellingShingle |
Snow Ice and Permafrost Civil Engineering (*SOILS DEFORMATION) (*PERMAFROST SOILS) FOUNDATIONS(STRUCTURES) CONSTRUCTION ICE MELTING FREEZING MOISTURE TABLES(DATA) SIBERIA USSR TRANSLATIONS Dubikov,G. I. Possible Settling of Perennially Frozen Loose Deposits in West Siberia during Thawing (Vozmoshnye Osadki pri Profaivanii Mnogelet Nemerzlykh Sibir) |
topic_facet |
Snow Ice and Permafrost Civil Engineering (*SOILS DEFORMATION) (*PERMAFROST SOILS) FOUNDATIONS(STRUCTURES) CONSTRUCTION ICE MELTING FREEZING MOISTURE TABLES(DATA) SIBERIA USSR TRANSLATIONS |
description |
In the development of land with perennially frozen friable deposits of great depth, a serious danger is presented by the thermal settlings of buildings erected on high-ice soils. Therefore a knowledge of the amounts of possible settlings permits the builder to form a rough judgment concerning the suitability or unsuitability of soils as a foundation for construction and to recommend a building technique even during the initial stage of studies. Since during thawing, the settlings are determined by the extent of ice saturation of the frozen friable deposits, while iciness is linked largely with the lithological composition and method of freezing the soils, the values of possible settlings also depend on these factors. The report gives values of possible settlings during the thawing of the upper levels of frozen Quaternary deposits in Western Siberia. (Author) Draft trans. of Merzlotnye Issledovaniya (USSR) n10 p220-222 1970. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
Dubikov,G. I. |
author_facet |
Dubikov,G. I. |
author_sort |
Dubikov,G. I. |
title |
Possible Settling of Perennially Frozen Loose Deposits in West Siberia during Thawing (Vozmoshnye Osadki pri Profaivanii Mnogelet Nemerzlykh Sibir) |
title_short |
Possible Settling of Perennially Frozen Loose Deposits in West Siberia during Thawing (Vozmoshnye Osadki pri Profaivanii Mnogelet Nemerzlykh Sibir) |
title_full |
Possible Settling of Perennially Frozen Loose Deposits in West Siberia during Thawing (Vozmoshnye Osadki pri Profaivanii Mnogelet Nemerzlykh Sibir) |
title_fullStr |
Possible Settling of Perennially Frozen Loose Deposits in West Siberia during Thawing (Vozmoshnye Osadki pri Profaivanii Mnogelet Nemerzlykh Sibir) |
title_full_unstemmed |
Possible Settling of Perennially Frozen Loose Deposits in West Siberia during Thawing (Vozmoshnye Osadki pri Profaivanii Mnogelet Nemerzlykh Sibir) |
title_sort |
possible settling of perennially frozen loose deposits in west siberia during thawing (vozmoshnye osadki pri profaivanii mnogelet nemerzlykh sibir) |
publishDate |
1972 |
url |
http://www.dtic.mil/docs/citations/AD0738127 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0738127 |
long_lat |
ENVELOPE(158.683,158.683,68.500,68.500) |
geographic |
Sibir’ |
geographic_facet |
Sibir’ |
genre |
Ice permafrost Siberia |
genre_facet |
Ice permafrost Siberia |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0738127 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027324501786624 |